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Climate change impact, mitigation and adaptation strategies for agricultural and water resources, in Ganga Plain (India)

机译:印度甘加平原的气候变化对农业和水资源的影响,缓解和适应战略

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Agriculture consumes more than two-thirds of global fresh water out of which 90 % is used by developing countries. Freshwater consumption worldwide is expected to rise another 25 %by 2030 due to increase in population from 6.6 billion currently to about 8 billion by 2030 and over 9 billion by 2050. Worldwide climate change and variability are affecting water resources and agricultural production and in India Ganga Plain region is one of them. Hydroclimatic changes are very prominent in all the regions of Ganga Plain. Climate change and variability impacts are further drying the semi-arid areas and may cause serious problem of water and food scarcity for about 250 million people of the area. About 80 million ha out of total 141 million ha net cultivated area of India is rainfed, which contributes approximately 44 % of total food production has been severely affected by climate change. Further changing climatic conditions are causing prominent hydrological variations like change in drainage density, river morphology (tectonic control) & geometry, water quality and precipitation. Majority of the river channels seen today in the Ganga Plain has migrated from their historic positions. Large scale changes in land use and land cover pattern, cropping pattern, drainage pattern and over exploitation of water resources are modifying the hydrological cycle in Ganga basin. The frequency of floods and drought and its intensity has increased manifold. Ganga Plain rivers has changed their course with time and the regional hydrological conditions shows full control over the rates and processes by which environments geomorphically evolve. Approximately 47 % of total irrigated area of the country is located in Ganga Plain, which is severely affected by changing climatic conditions. In long run climate change will affect the quantity and quality of the crops and the crop yield is going to be down. This will increase the already high food inflation in the country. The warmer atmospheric temperatures and drought conditions will increase soil salinization, desertification and drying-up of aquifer, while flooding conditions will escalate soil erosion, soil degradation and sedimentation. The aim of this study is to understand the impact of different hydrological changes due to climatic conditions and come up with easily and economically feasible solutions effective in addressing the problem of water and food scarcity in future.
机译:农业消耗了全球三分之二的淡水,其中90%被发展中国家使用。到2030年,由于人口将从目前的66亿增加到2030年的约80亿,到2050年将超过90亿,全球淡水消耗量预计将再增加25%。全球气候变化和多变性正在影响水资源和农业生产以及印度平原地区就是其中之一。在恒河平原的所有地区,水文气候变化非常明显。气候变化和多变性的影响使半干旱地区进一步干燥,并可能导致该地区约2.5亿人严重缺水和缺粮。在印度1.41亿公顷净耕地中,约有8000万公顷为雨养,占气候变化严重影响了粮食总产量的44%。气候条件的进一步变化导致显着的水文变化,例如排水密度,河流形态(构造控制)和几何形状,水质和降水的变化。今天在恒河平原上看到的大多数河道已经从其历史位置迁移了。土地利用和土地覆盖格局,耕作模式,排水模式和水资源过度开采的大规模变化正在改变恒河盆地的水文循环。洪水和干旱的频率及其强度在不断增加。恒河平原河流随着时间的流逝而改变了方向,区域水文条件显示出对环境地貌演化速率和过程的完全控制。该国大约47%的灌溉面积位于甘加平原,该地区受到气候条件变化的严重影响。从长远来看,气候变化将影响农作物的数量和质量,农作物的产量将下降。这将增加该国本已很高的食品通胀。较高的大气温度和干旱条件将增加土壤盐碱化,沙漠化和含水层的干燥,而洪水条件将加剧土壤侵蚀,土壤退化和沉积。这项研究的目的是了解由于气候条件而引起的不同水文变化的影响,并提出有效且经济可行的解决方案,以有效解决未来的水和粮食短缺问题。

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